{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1390282681489734656.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/bf03353017"}},{"identifier":{"@type":"COI","@value":"1:CAS:528:DC%2BD38XjtVKjtb4%3D"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"6262918"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/6262918"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I6262918"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/8838684"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/BF03353017.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/BF03353017/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/BF03353017"}},{"identifier":{"@type":"NAID","@value":"10008634519"}},{"identifier":{"@type":"NAID","@value":"130003956294"}}],"dc:title":[{"@language":"en","@value":"Degassing activity from Iwodake rhyolitic cone, Satsuma-Iwojima volcano, Japan: Formation of a new degassing vent, 1990-1999"},{"@value":"Degassing activity from Iwodake rhyolitic cone, Satsuma-Iwajima volcano, Japan: Formation of a new degassing vent, 1990-1999"},{"@value":"Degassing activity from Iwodake rhyolitic cone, Satsuma-Iwojima volcano, Japan: Formation of new degassing vent, 1990–1999: Earth"},{"@value":"Degassing activity from Iwodakerhyolitic cone, Satsuma-Iwojima volcano, Japan: formation of new degassing vent, 1990–1999"},{"@value":"Satsuma-Iwojima volcano, Japan: formation of a new degassing vent, 1990–1999"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Large changes in the surface manifestation of degassing activity were observed from 1990 to 1999 at the summit crater of Iwodake cone of Satsuma-Iwojima volcano. During this period, a new high-temperature fumarolic area formed in the center of the crater floor and became a degassing vent with a diameter of 40 m. Altered volcanic rocks were ejected during the course of vent formation. Although glass fragments were observed in the ejected ash, the glass comes from altered Iwodake rhyolite that covers the crater floor. The highest fumarolic temperature and equilibrium temperatures of volcanic gases had a maximum of about 900°C at the beginning of the vent formation. The flux of SO<SUB>2</SUB>, measured by COSPEC, varied from 300 to 700 ton/day and correlated directly with maximum fumarole temperature. During this period, open fractures formed along the southern rim of the crater almost contemporaneously with the vent formation and changes in the nature of fumarolic discharges. The continuous and intense degassing at Satsuma-Iwojima is likely caused by volatile transport from a deep magma chamber through a convecting magma column. An increase in the magma convection rate might have caused these large changes in surface manifestations, including increase in the SO<SUB>2</SUB> flux and fumarolic temperatures, ground deformation, and the vent formation."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410001204230607618","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000000767681"},{"@type":"NRID","@value":"9000254579584"},{"@type":"NRID","@value":"9000254740606"},{"@type":"NRID","@value":"9000004594076"},{"@type":"NRID","@value":"9000254740597"},{"@type":"NRID","@value":"9000254579056"},{"@type":"NRID","@value":"9000025118067"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0005357"}],"foaf:name":[{"@language":"en","@value":"Shinohara Hiroshi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geological Survey of Japan, 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Nobuo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geological Survey of Japan, AIST"}]},{"@id":"https://cir.nii.ac.jp/crid/1030848083686355202","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60356847"},{"@type":"NRID","@value":"1000060356847"},{"@type":"NRID","@value":"9000000767691"},{"@type":"NRID","@value":"9000017544887"},{"@type":"NRID","@value":"9000000767774"},{"@type":"NRID","@value":"9000254740603"},{"@type":"NRID","@value":"9000254740610"},{"@type":"NRID","@value":"9000014420783"},{"@type":"NRID","@value":"9000004594164"},{"@type":"NRID","@value":"9000020595926"},{"@type":"NRID","@value":"9000283578074"},{"@type":"NRID","@value":"9000283578055"},{"@type":"NRID","@value":"9000001330633"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0157560"}],"foaf:name":[{"@language":"en","@value":"Kawanabe Yoshihisa"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geological Survey of Japan, 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日本火山学会、日本測地学会、日本惑星科学会"}],"prism:publicationDate":"2002","prism:volume":"54","prism:number":"3","prism:startingPage":"175","prism:endingPage":"185"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/6262918"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I6262918"},{"@id":"https://dl.ndl.go.jp/pid/8838684"},{"@id":"https://link.springer.com/content/pdf/10.1186/BF03353017.pdf"},{"@id":"https://link.springer.com/article/10.1186/BF03353017/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1186/BF03353017"}],"availableAt":"2002","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338805661696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Remote determinations on fumarole outlet temperatures in an eruptive 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volcano"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303186816","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"三宅島火山の連続脱ガスに伴う小噴火噴出物に含まれる玄武岩本質物から推測する火道内マグマプロセス"},{"@language":"en","@value":"Conduit Magma Process of Miyakejima Volcano Inferred from Basaltic Juvenile Materials in the Products of the Small Ash Eruptions during the Continuous Degassing"},{"@language":"ja-Kana","@value":"ミヤケジマ カザン ノ レンゾク ダツガス ニ トモナウ ショウフンカ フンシュツブツ ニ フクマレル ゲンブガン ホンシチブツ カラ スイソク スル カドウナイ マグマプロセス"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204551182464","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Helium isotopes at Satsuma-Iwojima volcano, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512977536","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Iodine isotope ratios and halide concentrations in fluids of the Satsuma-Iwojima volcano, Japan"},{"@value":"Iodine isotope ratio and halide concentrations in fluids of the Satuma-Iwojima volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512979328","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High SiF<SUB>4</SUB>/HF ratio detected in Satsuma-Iwojima volcano's plume by remote FT-IR observation"},{"@value":"High SiF4/HF ratio detected in Satsuma-Iwojima volcano's plume by remote FT-IR observation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513019136","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mafic-felsic magma interaction at Satsuma-Iwojima volcano, Japan: Evidence from mafic inclusions in rhyolites"},{"@value":"Mafic-felsic magma interaction at Satsuma−Iwojima volcano, Japan: evidence from mafic inclusions in rhyolites"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513020288","@type":"Article","relationType":["references","isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Degassing process of Satsuma-Iwojima volcano, Japan: Supply of volatile components from a deep magma chamber"},{"@value":"Degrassing process of Satuma-Iwojima volcano, Japan: Supply of volatile components from a deep magma chamber"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513022080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Volcanic activity of the Satsuma-Iwojima area during the past 6500 years"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513524608","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Heat discharge estimation using satellite remote sensing data on the Iwodake volcano in Satsuma-Iwojima, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513526528","@type":"Article","relationType":["references","isReferencedBy","cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evaluation of recent activity at Satsuma-Iwojima -Felt earthquake on June 8, 1996-"},{"@value":"Evaluation of recent activity at Satsuma-Iwojima —Felt earthquake on June 8, 1996—"},{"@value":"Evaluation of recent activity at Satsuma-Iwojima—Felt earthquake on June 8, 1996"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679528509312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geochemistry of volcanic gases and hot springs of Satsuma-Iwojima, Japan: Following Matsuo."}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489685248","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Deposition of trace elements from high temperature gases of Satsuma-Iwojima 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